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Proceedings of the Bath
Royal Literary
& Scientific Institution – Seventh Year in New Series
– 2003 – Chairman Robert Draper
HERSCHEL SOCIETY MEETING
Convener:
Richard Phillips FRAS, The Herschel Society.
THE FRENCH CONNEXION
– BETWEEN ENGLISH AND FRENCH MAP SURVEYS
Michael
Knowles, BRLSI Member, on 3 January 2003
Mankind’s
concept of the Earth has
progressed from the flat
to the spherical form through Pythagoras, Aristotle, Eratosthenes (who
measured its diameter) and Hipparchus up to the 17th Century.
Our
knowledge of the Earth has progressed
with exploration. The western limit of the ancient world was the island
of Ferro in the Canaries and from the time of Ptolemy (AD150) its most
western point was the basis of navigation with a longitude of
0º up to
the late 15th century. In 1634 Louis XIII ratified the Ferro prime
meridian as
passing 20º west of Paris though this was inaccurate.
The
ellipsoidal era began with Newton and
Huygens. Triangulation conceived by Tycho Brahe in the 16th century was
developed into a science and used to measure arcs by Willebrord van
Roijen Snell
in the 17th century.
In
1669 the French astronomer Jean Picard
measured an arc of 1.2º north of Paris. Results suggested that
the Earth was a prolate spheroid. In 1670 a decimal metric system based
on the virga (1 virga = 1/1000th part of one minute of arc along a
meridian
= 1.852 m. = 1/1000th of a nautical mile)(1) was published by Gabriel
Mouton, just after Picard published a similar idea.
The
Paris Observatory was built between
1668-73 and Jean-Dominique Cassini (Gian Domenico) was appointed its
first director by Louis XIV. A French expedition to Guyane in 1672
found that
a clock lost 2½ minutes per day near Equator which supported
the
ellipsoidal Earth theory. Isaac Newton published his Principia in 1687
which predicted an
oblate spheroid with the poles flattened by 1/230 of the equatorial
diameter
(modern value = 1/297). Around 1700 Cassini I and Cassini II extended
Picard’s arc to Dunkerque and Spain. This was used later for
the ‘Metre Survey’.
In
1724 the French Royal Academy of
Sciences sent the astronomer Louis Feulliee to Ferro to determine the
difference in longitude between Orchilla and the Paris Observatory.
Dedicated to resolving
the question of the form of the Earth, the Academy of Sciences sent
Pierre Bouguer and Charles-Marie de La Condamine to Peru in 1735 to
measure a degree on the prime meridian at the Equator and in 1736 a
second expedition went to
Lapland, led by Pierre-Louis Moreau de Maupertuis, to measure one
degree on the
meridian near the North Pole.
In
1745 Cassini III published the first
surveyed map of France,
revealing that the land area was about 10 per cent greater than had
been thought previously. The Jacobite rebellion of 1745 showed the need
for a military map of the United Kingdom and by order of George III an
initial survey covered SE England to Hastings and Dover.
Photograph
of
Hanger Hill Tower in 1880
from a published work:
by courtesy of Hanger Hill East Residents
Association  |
The Cross-Channel Connexion, commenced
in 1784 under Major-General Roy.
Triangulation began from Windsor Castle,
via Hanger
Hill Tower and St Ann’s Hill (Chertsey) across
Surrey,
Sussex and Kent to Hastings, Dymchurch and Dover Castle by 1787. The
project was
recorded by Roy in the Philosophical Transactions of the Royal Society
Vol XX
(1790) with diagrams of a Ramsden three-foot theodolite that was used
for angular
measurements.
The
original base-line across Hounslow Heath
was chosen in April 1784
between King’s Arbour and Hampton Poor House. In July-August
it was measured with deal rods and iron bars to be 27,404
ft. When it was re-measured with 1,370 placements of glass tubes as
27,406 ft.
When this was corrected for temperature and mean sea-level, the value
after
re-measurement by Mudge was 27,404.2 ft (i.e. 8.352800 km). This
accuracy of 1 inch in 27,404 ft is 3 parts per million.
Sightings
from the ends of the baseline to
St Ann’s Hill (Chertsey) and Hanger Hill Tower gave another
calculated baseline
for the triangulations to Severndroog Castle (near Greenwich) and
Hundred Acre
(Banstead), then quadrilaterals through Frant to Hastings (Fairlight
Down), and
Hollingbourne Hill (Maidstone) to Allington Knoll and Dover Castle.
Before
taking measurements to France, a
check-base was set up on Romney Marsh, West of Dymchurch, of
approximately
30,000 feet. The error of the value calculated by triangulation from
Hounslow
Heath baseline was alleged to be 1 foot (33 p.p.m.).
The
cross-channel observations were made in
September 1787 after the French party (Arago and Mathieu) had crossed
to Dover
by boat. Both parties enjoyed the cordial encounter, where a scientific
common
interest transcended national and political issues. A baseline was set
up on
the French coast East of Dunkirk but measured with deal rods. The
English
measurements connected with French stations of the Cassini survey at
Montlambert,
Calais (Notre Dame) and Dunkerque (Tower). Point M is between the
latter
stations. The French Revolutionary Assembly adopted the new unit of
length, the
provisional metre, in 1791.
A
new survey, ordered and signed by Louis
XVI on 19th June 1792, was completed in 1798. Astronomers Jean-Baptiste
Delambre and Pierre Mechain left Paris to survey France north and south
of
Rodez on the basis of the triangulatlons of Cassinis II and III - a
century
earlier.
The
diagram of the northern triangulation from
Paris to Dunkirk, surveyed by J-B Delambre, was principally in flat
country and
shows the baseline near Amiens. Note that the unit of measurement was
the Toise
(fathom) of Peru.
The
diagram of the southern triangulation
by P F Mechain through the Pyrenees was in arduous country. The
baseline was
measured from Salces to Vernet near Perpignan. The Paris meridian
intersects
the Spanish coast at Premia del Mar, east of Barcelona. In December
1798 there
was a grand convention in Paris of the six original signatory nations
to the
Metric System. Mechain was plagued by realisation that one of his
surveys
contained an error.
The typical
instrument for observing two
heavenly bodies or objects was the 1805 ‘Repeating
Circle’ by Lenoir, with two
telescopes. Instruments used for surveying were heavier.
While the
metre survey was in progress,
the
first triangulation of Great Britain was undertaken from 1791 to 1822,
using
the new Ramsden theodolite and chains in lieu of deal rods or glass
tubes.
Baselines were at Hounslow Heath, Salisbury Plain, Sedgemoor, Misterton
Carr,
Clifton (Yorks), Belhevie Sands (North of Aberdeen) and Rhuddlan Marsh,
North
Wales. The Irish Survey was also undertaken by Colby, from his HQ in
Phoenix
Park, Dublin. Ireland was connected with the British Island across St
George’s
Channel and Irish Sea using limelight introduced by Major Drummond and
which
was visible by night at 67 miles.
The
Greenwich-Paris connexion was
re-measured in 1821-23 by Colby and Captain Henry Kater, who ignored
the work
of Roy and Mudge of 1784-87. The surveys in France were supervised by
Arago and
Mathieu. The Cross-Channel sightings were made over distances up to 48
miles
(77 km) with 3-ft limelights.
As
calculations were based on the
Bouguer
spheroid, the 1821-23 re-measurement was technically better than that
of Roy
and Mudge. Kater wrote his report before the French published their
results.
The difference of longitude between Greenwich and Paris was calculated
via
Calais (Notre Dame) as 2º 20' 10". The Greenwich physical
meridians of
Bradley, Pond and Airy were superceded by a virtual meridian following
satellite measurements in the 1970s.. The IGN value is 2º 20'
14.25".
No
historical account of the
Cross-Channel
Connexion would be complete without a mention of Alexander Ross Clarke.
He
attended the Royal Military Academy at Woolwich, joined HM Ordnance
Survey in
1850, and was appointed Head of Dept of Trigonometry and Levelling in
1856. In
1863, he led a new triangulation between England, France and Belgium
and made
determinations of the form of the Earth in 1858, 1866 and 1880, leading
to
publication of his book Geodesy in 1880.
Clarke’s
spheroid of 1866 was
used as the
basis of geodesy by triangulation in the United States, a gargantuan
task of
the early 20th century, undertaken by General Gordon Meade.
Meade’s Ranch
contains a stone marker, which was used as the datum for triangulation.
In
1927, it was adopted by Mexico & Canada and thus became the
geodetic centre
of North America.
Baseline
measurements and national
surveys
proliferated in the 19th century.
In 1824,
Austria based its cadastral
longitudes on the Ferro meridian. In 1832, the German mathematician F.
W.
Bessel measured a baseline and set up the observatory at Konigsberg.
The
Federal German survey is based on a national reference point at
Rauenberg near
Berlin (in Bavaria at Munich Marienkirche) and international reference
points
introduced with effect from 1991.
The French meridian and the Metre Survey
were celebrated in France at the Millennium, by the creation of "La
Meridienne Verte" - a line of trees planted along the historic axis.
This
was especially celebrated at the town of Clermont de 1'Oise, which is
very near
the meridian. A statue also commemorates Cassini III, i.e. Cesar
Francois Cassini
de Thury. The Cassini family tree shows a complete dynasty of French
astronomers. It extends over a century from the opening of the Paris
Observatory in 1672 and appointment of Cassini I.
The churches at Clermont, Noyers St
Martin
and Coivrel used as triangulation points now have new towers, new roofs
and
repairs of damage in WW2 which mask traces of the
astronomers’ visits, if any
remained.
The Orchilla lighthouse now stands on
Ferro
at Ptolemy’s meridian, an historic juxtaposition of two great
contributions to
the sciences of navigation and geodesy in the seventeenth century,
which one
may still inspect today.
A selection of documents was received
from
the Orchilla Lighthouse including photocopies from "El Hierro
– La Isla de
la Longitud"
Copyright Michael Knowles
&
Richard
Phillips © 2003
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